96707 feature ID 2627933 Kalaeloa is a (CDP) in, United States. The population was 48 at the. The community occupies the location of the former, which was closed in 1999 and subsequently transferred to the. The geographical name, Ka lae loa, means 'long point' in and is the native name for what is now called Barbers Point on. The area was known as Barbers Point because Captain wrecked his ship on a coral shoal at this location on October 31, 1796.
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In 1993, after the federal government listed Barbers Point for closure, the state legislature established the Barbers Point Naval Air Station Redevelopment Commission (BPNAS-RC) to guide the redevelopment of the former military facilities comprising John Rodgers airfield and 3,700 acres (15 km 2) of land along the south shore of Oʻahu between the towns of,, and Campbell Industrial Park. On July 1, 2002, the Hawaii Community Development Authority became the redevelopment authority for Kalaeloa.
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The former Naval Air Station runways and associated facilities are now. Barbers Point Housing is that part of Kalaeloa retained temporarily by the for housing. Contents • • • • • • • • Geography [ ] Kalaeloa is located at 21°19'28' North, 158°4'59' West (21.324550, -158.083156). Climate [ ] have monthly mean temperature above 18 °C (64 °F) in every month of the year and typically a pronounced dry season, with the driest month having precipitation less than 60mm (2.36 in) of precipitation. Retrieved January 31, 2008. • United States Postal Service (2012). Retrieved February 15, 2012.
Census Bureau, American Factfinder. Retrieved May 18, 2012. Retrieved 2011-04-23.
Retrieved on April 25, 2013. • Clark, John R.K (2002). Hawaii Place Names. United States of America: Mike Waggoner. • Duane Shimogawa (25 September 2013). Pacific Business News.
American City Business Journals. Retrieved 12 March 2015. • ^ Mykleseth, Kathryn (September 7, 2017).. Retrieved September 7, 2017. External links [ ] •.
Tilted bedrock in the walls of the main crater Kaali is a group of nine in the village of on the island of. Most recent estimates put its formation shortly after 1530–1450 BC (3237+/-10 14C yr BP). It was created by an and is one of the few impact events that has occurred in a populated area (other ones are: and ).
Before the 1930s there were several hypotheses about the origin of the crater, including theories involving and processes. Its meteoritic origins were first conclusively demonstrated by Ivan Reinvald in 1928, 1933 and 1937.